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14 results were found for WA 0821 1305 0400 Rencana Anggaran Biaya Renovasi Plafon Gypsum Wr Berpengalaman Jakarta Utara.


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  • 11. Journal_of_Hydrology_Veijalainen_etal

    The hydrological simulations were performed with the Wa- tershed Simulation and Forecasting System (WSFS) developed and operated in the Finnish Environment Institute (Vehviläinen et al., 2005). The WSFS is used in Finland for operational hydrolog- ical forecasting and flood warnings (www.environment.fi/water- forecast/), regulation planning and research purposes (Vehviläinen and Huttunen, 1997 /media/ces/Journal_of_Hydrology_Veijalainen_etal.pdf
  • 12. VI_2015_007

    rank was calculated and each model setup sorted accordingly: WR = 0:5Rank(NS AMF)+0:3Rank(NS Qd)+0:2Rank(NS E[Qd]) (10) Next, the best model run was selected and validated on a different period than the calibration pe- riod. Results of the calibration and validation periods are summarized in Tables 5 and 6 and Ap- pendix II. Overall, WaSiM model simulations compare quite well with observations /media/vedurstofan/utgafa/skyrslur/2015/VI_2015_007.pdf
  • 13. Hare-2011-ParticipatoryModelling

    ea th , th e m et ho d u se d at th is st ag e fo r th es e st ak eh o ld er typ es is sp ec ied .Sh oul d ther e be tw o o r mor e model sbein g develope d in th e process ,the n th e typ e o fmode lt o whic h th e metho d wa s applie d is show n in parentheses .O T re fe rs to th e co m po si tio n o ft he o rg an iz in g te am . Fo r o rg an iz in g te am in vo lve m en t in di ffe re n t pa rt /media/loftslag/Hare-2011-ParticipatoryModelling.pdf
  • 14. VI_2009_006_tt

    than can be expected to originate from the cauldrons, three to four times the wa- ter equivalent of the accumulation of snow over the watershed of the cauldrons. It has been estimated that flow from the cauldrons, in addition to the jökulhlaups, could be 2–5 m3 s 1 at maximum (Vatnaskil, 2005). It is possible that part of the sulfate-rich groundwater from the glacier comes from the cauldrons /media/vedurstofan/utgafa/skyrslur/2009/VI_2009_006_tt.pdf

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